Heed fresh snowdrifts. Isolated danger zones in gullies and bowls.
Fresh snowdrift accumulations are mostly small, triggerable only in isolated cases, esp. on wind-protected shady slopes at high altitude. Caution urged in transitions into gullies and bowls. These danger zones occur seldom.
Snowpack
Freshly generated snowdrift accumulations have been deposited on top of an unfavorable old snowpack surface.
Tendency
Pay attention to fresh snowdrifts
Danger level
2400m
Avalanche Problem
Persistent weak layer
2400m
Wind slab
2400m
Caution: isolated weak layers prone to triggering. Heed drifts.
Weak layers in the old snow can be triggered in many cases by one sole skier on W/N/E facing slopes above 2400m. Caution in transitions from shallow to deeper snow, e.g. at entry points into gullies and bowls. Due to fresh snow and northerly winds, trigger-sensitive snowdrift accumulations were generated in gullies, bowls and behind protruberances in the landscape. They can be triggered by one sole skier in the weak old snow, esp. on W/N/E facing slopes above 2400m. Danger zones are easy to recognize for the practiced eye. Avalanches can reach medium size.
Snowpack
dp.6: cold, loose snow and wind dp.4: cold following warm / warm following cold
In the lowermost part of the snowpack there are faceted, expansively metamorphosed weak layers, esp. on W/N/E facing slopes. The fresh snowdrift accumulations lie deposited atop an unfavorable old snowpack surface in high-alpine zones. Highly varied snow depths, depending on wind impact.
Tendency
Fresh snowdrifts need to be cautiously assessed. Pay attention to weak layers in old snowpack.
Danger level
2000m
Avalanche Problem
Persistent weak layer
2000m
Heed weak layers in the old snow
Weak layers in the old snow can be triggered in many cases by one sole skier on NW/N/E facing slopes esp. above 2000m. Caution in transitions from shallow to deeper snow, e.g. at entry points into gullies and bowls. Due to fresh snow and northerly winds, trigger-sensitive snowdrift accumulations were generated in gullies, bowls and behind protruberances in the landscape. Avalanches can reach medium size.
Snowpack
dp.1: deep persistent weak layer dp.4: cold following warm / warm following cold
At mid-level inside the snowpack, esp. on N/NW/NE facing slopes where the snow is shallow, faceted, espansively metamorphosed weak layers are evident. The snowpack is highly diverse even over small areas.
Tendency
Assess snowdrifts with caution
Danger level
2200m
Avalanche Problem
Persistent weak layer
2200m
Heed weak layers in the old snow, they can be triggered in isolated cases
Weak layers in the old snow can be triggered in many cases by one sole skier on W/N/E facing slopes above 2200m. Caution in transitions from shallow to deeper snow, e.g. at entry points into gullies and bowls. Avalanches can reach medium size.
Snowpack
dp.4: cold following warm / warm following cold dp.1: deep persistent weak layer
Inside the snowpack, esp. on N/NW/NE facing slopes where the snow is shallow, faceted, espansively metamorphosed weak layers are evident. The snowpack is highly diverse even over small areas.